Sulfide Immiscibility in the Lunar Magma Ocean: Evidence for a Primitive Lunar Lower Mantle and the Origin of High-µ Mare Basalts

Details Sulfide Immiscibility in the Lunar Magma Ocean: Evidence for a Primitive Lunar Lower Mantle and the Origin of High-µ Mare Basalts Sulfide Immiscibility in the Lunar Magma Ocean: Evidence for a Primitive Lunar Lower Mantle and the Origin of High-µ Mare Basalts

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.1821n&link_type=abstract

33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.1821

Physics

Scientific paper

Chalcophile, lithophile, and highly siderophile elements are used to
examine the source of mare volcanic products. The lunar magma ocean
experienced extraction of an immiscible sulfide liquid during its
crystallization. This accounts for the extreme high-µ values
exhibited by mare basalts.

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